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| 云南砚山红舍克原生及堆积型铝土矿 | |
| 引用本文： | 刘汉和. 云南砚山红舍克原生及堆积型铝土矿[J]. 云南地质, 2007, 26(1): 32-40 |
| 作者姓名： | 刘汉和 |
| 作者单位： | 云南省有色地质勘查院曲靖院,云南,曲靖,655000 |
| 摘 要： | 红舍克铝土矿分为沉积和堆积型两类,受上二叠统(P2l)含矿层控制明显:沉积矿位于上段(P2l2)下部,堆积矿位于沉积铝土矿上覆层。 |
| 关 键 词： | 铝土矿 沉积及堆积型 成因探讨 砚山云南 |
| 文章编号： | 1004-1885（2007）-032-09 |
| 收稿时间： | 2006-08-14 |
| 修稿时间： | 2006-08-14 |
HONGSHEKE ORIGINAL AND SECONDARY BAUXITE DEPOSITIN YANSHAN, YUNNAN |
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| LIU Han-he. HONGSHEKE ORIGINAL AND SECONDARY BAUXITE DEPOSITIN YANSHAN, YUNNAN[J]. Yunnan Geology, 2007, 26(1): 32-40 | |
| Authors: | LIU Han-he |
| Affiliation: | Qujing Branch, Yunnan Nonferrous Geoexploration Institute, Qujing 655000 |
| Abstract: | This bauxite deposit can be divided into 2 types of sedimentation and accumulation,which are controlled evidently by the Upper Permian(P2l) ore-bearing bed.The former type ore deposit is in the lower part of Upper Permian Upper Member(P2l2);the latter one is in the Quaternary accumula tion horizon near the sedimentary type bauxite deposit. |
| Keywords: | Bauxite Sedimentation and Accumulation Types Genesis Discussion Yanshan Yunnan |
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